labarai

Babban bangaren diatomaceous ƙasa a matsayin mai ɗauka shine SiO2. Misali, sashin aiki na masana'antar vanadium mai kara kuzari shine V2O5, mai talla shine alkali karfe sulfate, kuma mai ɗaukar kaya yana da tsabtace ƙasa diatomaceous. Gwaje-gwaje sun nuna cewa SiO2 yana da tasiri mai ƙarfi akan abubuwan da ke aiki, kuma yana ƙarfafawa tare da haɓakar K2O ko Na2O abun ciki. Har ila yau, aikin mai kara kuzari yana da alaƙa da tarwatsawar pore tsarin motar

ina. Bayan an bi da diatomite tare da acid, an rage ƙazantaccen abun ciki na oxide, abun ciki na SiO2 ya karu, kuma ƙayyadaddun yanki da girman pore kuma suna karuwa. Sabili da haka, tasirin mai ɗaukar nauyin diatomite mai ladabi ya fi na diatomite na halitta.

Duniyar diatomaceous gabaɗaya tana samuwa ne ta ragowar silicate bayan mutuwar algae mai sel guda ɗaya da ake kira diatoms, kuma ainihinsa shine SiO2 mai ɗauke da ruwa. Diatoms na iya rayuwa a cikin ruwa mai daɗi da ruwan gishiri. Akwai nau'ikan diatoms da yawa. Gabaɗaya, ana iya raba su zuwa “tsakiyar oda” diatoms da “tsarin oda” diatoms. A cikin kowane tsari, akwai “jinus” da yawa, waɗanda ke da rikitarwa.

Babban bangaren na halitta diatomaceous duniya shine SiO2, masu inganci masu inganci fari ne, kuma abun ciki na SiO2 yakan wuce 70%. Monomer diatoms ba su da launi kuma masu gaskiya. Launin duniya diatomaceous ya dogara da ma'adinan yumbu da kwayoyin halitta. Abubuwan da ke tattare da diatoms akan ma'adanai daban-daban sun bambanta.

Diatomaceous Earth shine burbushin diatomaceous diatomaceous ajiya da aka samu bayan mutuwar wani tsiro mai kwayar halitta da ake kira diatom bayan tarawa na kimanin shekaru 10,000 zuwa 20,000. Diatoms suna ɗaya daga cikin protists na farko da suka bayyana a duniya, suna zaune a cikin ruwan teku ko ruwan tafkin. Wannan diatom ne ke ba da iskar oxygen ga ƙasa ta hanyar photosynthesis kuma yana haɓaka haihuwar mutane, dabbobi da tsirrai.